dolomitization

Crystalline dolostone is formed by seepage - reflux dolomitization and burial dolomitization.

晶粒白云岩有两种成因:一为回流渗透白云石化;二为深埋藏白云石化.

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The diageneses which are constructive to the reservoirs are mainly dolomitization and burial dissolution.

对储层起建设性作用的成岩作用主要有白云石化作用、埋藏溶解作用.

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The dolomitization is dominated by mixed water dolomitization in the diagenetic stage, followed by burial dolomitization.

白云石化作用,以早成岩阶段混合水白云石化作用为主, 埋藏白云石化作用次之.

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